{"id":74296,"date":"2005-03-06T00:00:00","date_gmt":"2005-03-06T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/utilizacion-del-analisis-pola%c2%adnico-para-la-reconstruccion-de-la-vegetacion-clima-y-estimacion-de-paleoaltitudes-a-lo-largo-del-arco-alpino-europeo-durante-el-mioceno-21-8-ma\/"},"modified":"2005-03-06T00:00:00","modified_gmt":"2005-03-06T00:00:00","slug":"utilizacion-del-analisis-pola%c2%adnico-para-la-reconstruccion-de-la-vegetacion-clima-y-estimacion-de-paleoaltitudes-a-lo-largo-del-arco-alpino-europeo-durante-el-mioceno-21-8-ma","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/utilizacion-del-analisis-pola%c2%adnico-para-la-reconstruccion-de-la-vegetacion-clima-y-estimacion-de-paleoaltitudes-a-lo-largo-del-arco-alpino-europeo-durante-el-mioceno-21-8-ma\/","title":{"rendered":"Utilizaci\u00f3n del an\u00e1lisis pol\u00ednico para la reconstrucci\u00f3n de la vegetaci\u00f3n, clima y estimaci\u00f3n de paleoaltitudes a lo largo del arco alpino europeo durante el mioceno 21-8 ma."},"content":{"rendered":"<h2>Tesis doctoral de <strong> Gonzalo Jim\u00e9nez Moreno <\/strong><\/h2>\n<p>Se ha realizado un an\u00e1lisis palinol\u00f3gico en numerosas localidades del mioceno (21-8 ma) del arco alpino europeo, con el objeto principal de la reconstrucci\u00f3n de la vegetaci\u00f3n y del clima y su evoluci\u00f3n. Se ha observado una degradaci\u00f3n progresiva de la vegetaci\u00f3n y del clima durante el mioceno en europa, que se confirma por la las estimaciones de los par\u00e1metros clim\u00e1ticos a partir de los datos de polen y se interpreta como producto del enfriamiento clim\u00e1tico progresivo ocurrido bajo el efecto de una glaciaci\u00f3n ant\u00e1rtica y de la tect\u00f3nica alpina. A partir de los datos de polen se han podido caracterizar, un gradiente clim\u00e1tico latitudinal en el sw de europa y cambios clim\u00e1ticos en relaci\u00f3n con ciclos de milanikovitch. La paleoaltitud de los relieves relacionados con las cuencas sedimentarias muestran el levantamiento progresivo del arco alpino europeo durante el mioceno.  finalmente, el an\u00e1lisis de los dinoflagelados ha permiti\u00f3 la construcci\u00f3n de una biozonaci\u00f3n para el paratethys central.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Utilizaci\u00f3n del an\u00e1lisis pol\u00ednico para la reconstrucci\u00f3n de la vegetaci\u00f3n, clima y estimaci\u00f3n de paleoaltitudes a lo largo del arco alpino europeo durante el mioceno 21-8 ma.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Utilizaci\u00f3n del an\u00e1lisis pol\u00ednico para la reconstrucci\u00f3n de la vegetaci\u00f3n, clima y estimaci\u00f3n de paleoaltitudes a lo largo del arco alpino europeo durante el mioceno 21-8 ma. <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Gonzalo Jim\u00e9nez Moreno <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Granada<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 03\/06\/2005<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n<h3>Direcci\u00f3n y tribunal<\/h3>\n<ul>\n<li><strong>Director de la tesis<\/strong>\n<ul>\n<li>Pascual Rivas Carrera<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Juan  Carlos Braga alarcon <\/li>\n<li>volker Mosburgger (vocal)<\/li>\n<li>pascal Allemand (vocal)<\/li>\n<li>  (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Gonzalo Jim\u00e9nez Moreno Se ha realizado un an\u00e1lisis palinol\u00f3gico en numerosas localidades del mioceno (21-8 ma) del [&hellip;]<\/p>\n","protected":false},"author":1,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"site-sidebar-layout":"default","site-content-layout":"","ast-site-content-layout":"","site-content-style":"default","site-sidebar-style":"default","ast-global-header-display":"","ast-banner-title-visibility":"","ast-main-header-display":"","ast-hfb-above-header-display":"","ast-hfb-below-header-display":"","ast-hfb-mobile-header-display":"","site-post-title":"","ast-breadcrumbs-content":"","ast-featured-img":"","footer-sml-layout":"","theme-transparent-header-meta":"","adv-header-id-meta":"","stick-header-meta":"","header-above-stick-meta":"","header-main-stick-meta":"","header-below-stick-meta":"","astra-migrate-meta-layouts":"default","ast-page-background-enabled":"default","ast-page-background-meta":{"desktop":{"background-color":"var(--ast-global-color-4)","background-image":"","background-repeat":"repeat","background-position":"center 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